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From: "Gotham Steel Grill Cooks" <Contact@grsulltra.us>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Love Burgers & Dogs, But Hate Grilling Outside?
Date: Tue, 21 Aug 2018 15:21:42 +0200
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Content preview:  Love Burgers & Dogs, But Hate Grilling Outside? http://grsulltra.us/Z0BpWkSy0no_tWv7vhxC0v_Nf7DyT8mdt_4a7sy3ZSVIlHMj_4698_2070_c87d8a7a_0300
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Date: Tue, 21 Aug 2018 15:21:42 +0200
From: "Gotham Steel Grill Cooks" <Contact@grsulltra.us>
Reply-To: "Own Gotham Steel Grill" <Support@grsulltra.us>
Subject: Love Burgers & Dogs, But Hate Grilling Outside?
To: <christian.gabriel@ift-informatik.de>
Message-ID: <8b7hk2wbb2wqh8sa-ib89cmyyxd141yv0-2070-125a@grsulltra.us>

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Love Burgers & Dogs, But Hate Grilling Outside?

http://grsulltra.us/Z0BpWkSy0no_tWv7vhxC0v_Nf7DyT8mdt_4a7sy3ZSVIlHMj_4698_2070_c87d8a7a_0300

http://grsulltra.us/77VN-IBPwB7bxv-AoMllqfWh9uoSb_Kyel9OMu6lq1C8zk4_4698_2070_c078c42f_0300

Climate in the mountains becomes colder at high elevations, due an interaction between radiation and convection. Sunlight in the visible spectrum hits the ground and heats it. The ground then heats the air at the surface. If radiation were the only way to transfer heat from the ground to space, the greenhouse effect of gases in the atmosphere would keep the ground at roughly 333 K (60 °C; 140 °F), and the temperature would decay exponentially with height.However, when air is hot, it tends to expand, which lowers its density. Thus, hot air tends to rise and transfer heat upward. This is the process of convection. Convection comes to equilibrium when a parcel at air at a given altitude has the same density as its surroundings. Air is a poor conductor of heat, so a parcel of air will rise and fall without exchanging heat. This is known as an adiabatic process, which has a characteristic pressure-temperature dependence. As the pressure gets lower, the temperature decreases. The rate of decrease of temperature with elevation is known as the adiabatic lapse rate, which is approximately 9.8 °C per kilometer (or 5.4 °F per 1000 feet) of altitude.Note that the presence of water in the atmosphere complicates the process of convection. Water vapor contains latent heat of vaporization. As air rises and cools, it eventually becomes saturated and cannot hold its quantity of water vapor. The water vapor condenses (forming clouds), and releases heat, which changes the lapse rate from the dry adiabatic lapse rate to the moist adiabatic lapse rate (5.5 °C per kilometer or 3 °F per 1000 feet) The actual lapse rate can vary by altitude and by location.Therefore, moving up 100 meters on a mountain is roughly equivalent to moving 80 kilometers (45 miles or 0.75° of latitude) towards the nearest pole. This relationship is only approximate, however, since local factors such as proximity to oceans (such as the Arctic Ocean) can drastically modify the climate. As the altitude increases, the main form of precipitation becomes snow and the winds increase.

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	<title>gotham steel</title>
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<p style="color:#ffffff">Climate in the mountains becomes colder at high elevations, due an interaction between radiation and convection. Sunlight in the visible spectrum hits the ground and heats it. The ground then heats the air at the surface. If radiation were the only way to transfer heat from the ground to space, the greenhouse effect of gases in the atmosphere would keep the ground at roughly 333 K (60 &deg;C; 140 &deg;F), and the temperature would decay exponentially with height.However, when air is hot, it tends to expand, which lowers its density. Thus, hot air tends to rise and transfer heat upward. This is the process of convection. Convection comes to equilibrium when a parcel at air at a given altitude has the same density as its surroundings. Air is a poor conductor of heat, so a parcel of air will rise and fall without exchanging heat. This is known as an <a href="http://grsulltra.us/HMB5V454LKm7cZBAoXCbJnPa2Hw3KBH2jzz0XdYjdMD_Gw_4698_2070_9af8a6f8_0300"><img src="http://grsulltra.us/c77df3fb471f23ae88.jpg" /><img height="1" src="http://www.grsulltra.us/OFONqXh1sf0LDyyBMvI1xdZfP1y_CdkolunxYPgos4aW-kY_4698_2070_9f517878_0300" width="1" /></a>adiabatic process, which has a characteristic pressure-temperature dependence. As the pressure gets lower, the temperature decreases. The rate of decrease of temperature with elevation is known as the adiabatic lapse rate, which is approximately 9.8 &deg;C per kilometer (or 5.4 &deg;F per 1000 feet) of altitude.Note that the presence of water in the atmosphere complicates the process of convection. Water vapor contains latent heat of vaporization. As air rises and cools, it eventually becomes saturated and cannot hold its quantity of water vapor. The water vapor condenses (forming clouds), and releases heat, which changes the lapse rate from the dry adiabatic lapse rate to the moist adiabatic lapse rate (5.5 &deg;C per kilometer or 3 &deg;F per 1000 feet) The actual lapse rate can vary by altitude and by location.Therefore, moving up 100 meters on a mountain is roughly equivalent to moving 80 kilometers (45 miles or 0.75&deg; of latitude) towards the nearest pole. This relationship is only approximate, however, since local factors such as proximity to oceans (such as the Arctic Ocean) can drastically modify the climate. As the altitude increases, the main form of precipitation becomes snow and the winds increase.</p>
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